The Riverland is Australia’s largest winegrape region by tonnage produced. It is located north-east of the city of Adelaide, about 200km inland. The climate is Continental – long sunny days give way to noticeably cooler nights.
The GI region is 4105 km2 in size and has a total of 22,032 hectares of vineyards. The main varieties grown in the region are Shiraz, Chardonnay, and Cabernet Sauvignon.
Riverland Regional Snapshot 2020-2021
Regional Snapshots are one-page profiles updated annually of individual Australian wine regions. They provide at-a-glance summary statistics on: climatic characteristics, viticulture data, winegrape production, and winegrape price and export sales data for wine, compared against the same statistics for the whole of Australia.
Download nowAlternative Varieties
From Arneis to Zinfandel: As the region continues to grow and adapt to new conditions, grape growers and winemakers continue to explore new grape varieties with the view to delivering high-quality and delicious wines. Southern Mediterranean varieties such as Montepulciano, Vermentino and Nero d’Avola are showing real promise.
Cabernet Sauvignon and Merlot
Cabernet Sauvignon and Merlot are also grown extensively. Each is used as single varietal wines and in blends. The region’s warm temperatures tend to bring out the richer raspberry characteristics in the wines, while in cooler years the overall profile can demonstrate mint and blackcurrant.
Chardonnay
The Riverland boasts more Chardonnay plantings than the combined total of other regions in South Australia. Riverland Chardonnay often exhibits vivacious and ripe flavours. Oak is often used, and this supports the richness of the wines as well as adding further complexity.
- The Riverland climate is Continental, resulting in long sunny days and noticeably cooler nights.
- Long sunshine hours ensure fruit ripens fully and low relative humidity results in little or no disease pressures.
- The soils of the Riverland vary significantly. The two main types are river valley soils, consisting of sandy loams over clay subsoils, and Mallee soils on higher ground, consisting of wind-blown sands over lime and clay layers.
- Soils within the river valley, comprising loams and clays, were formed when fine clay and silt particles were deposited over the flood plain by the River Murray.
- On higher ground, the Mallee landscape is characterized by depressions and rises and consists of windblown sands over lime and clay layers.